Larom, DGarstang, MLindeque, MRaspet, RZunckel, MHong, YBrassel, KOBeirne, SSokolic, F2007-03-282007-06-072007-03-282007-06-071997-03Larom, D, et al. 1997. Meteorology and elephant infrasound at Etosha National Park, Namibia. Journal of Acoustical society of America, vol. 101(3), pp 1710-17170001-4966http://hdl.handle.net/10204/2145http://hdl.handle.net/10204/2145Measured vertical profiles of temperature and wind an used to model infrasound propagation over a representative high savanna habitat typically occupied by the African elephant, Loxodonta Africana, to predict calling distance and area as a function of the meteorological variables, The profiles were measured up to 300 m above the surface by tethered balloon-borne instruments in Etosha National Park, Namibia, during the late dry season. Continuous local surface layer measurements of wind and temperature at 5 and 10 m provide the context for interpreting the boundary layer profiles. The fast field program (FFP) was used to predict the directionally dependent attenuation of a 15-Hz signal under these measured atmospheric conditions, the attenuation curves are used to estimate elephant infrasonic calling range and calling area, Directionality and calling range are shown to be controlled by the diurnal cycle in wind (shear) and temperature. Low-level nocturnal radiative temperature inversions and low surface wind speeds make the early evening the optimum time for the transmission of low-frequency sound at Etosha, with range at a maximum and directionality at a minimum, As the night progresses, a nocturnal low-level wind maximum (jet) forms, reducing upwind range and calling area, The estimated calling area drops rapidly after sunrise with the destruction of the inversion, Daytime calling areas are usually less than 50 km(2), while early evening calling areas frequently exceed 200 km(2) and are much less directional, This marked diurnal cycle will be present in any dry savanna climate, with variations due to local topography and climate, Calling range and low-frequency sound propagation cannot be effectively understood without knowledge of meteorological controls190439 bytesapplication/pdfenCopyright: 1997 Acoustical Society of AmericaElephant infrasound propagationAfrican ElephantsBoundary layer profilesEstosha National ParkNamibiaArticleLarom, D., Garstang, M., Lindeque, M., Raspet, R., Zunckel, M., Hong, Y., ... Sokolic, F. (1997). Meteorology and elephant infrasound at Etosha National Park, Namibia. http://hdl.handle.net/10204/2145Larom, D, M Garstang, M Lindeque, R Raspet, M Zunckel, Y Hong, K Brassel, S OBeirne, and F Sokolic "Meteorology and elephant infrasound at Etosha National Park, Namibia." (1997) http://hdl.handle.net/10204/2145Larom D, Garstang M, Lindeque M, Raspet R, Zunckel M, Hong Y, et al. Meteorology and elephant infrasound at Etosha National Park, Namibia. 1997; http://hdl.handle.net/10204/2145.TY - Article AU - Larom, D AU - Garstang, M AU - Lindeque, M AU - Raspet, R AU - Zunckel, M AU - Hong, Y AU - Brassel, K AU - OBeirne, S AU - Sokolic, F AB - Measured vertical profiles of temperature and wind an used to model infrasound propagation over a representative high savanna habitat typically occupied by the African elephant, Loxodonta Africana, to predict calling distance and area as a function of the meteorological variables, The profiles were measured up to 300 m above the surface by tethered balloon-borne instruments in Etosha National Park, Namibia, during the late dry season. Continuous local surface layer measurements of wind and temperature at 5 and 10 m provide the context for interpreting the boundary layer profiles. The fast field program (FFP) was used to predict the directionally dependent attenuation of a 15-Hz signal under these measured atmospheric conditions, the attenuation curves are used to estimate elephant infrasonic calling range and calling area, Directionality and calling range are shown to be controlled by the diurnal cycle in wind (shear) and temperature. Low-level nocturnal radiative temperature inversions and low surface wind speeds make the early evening the optimum time for the transmission of low-frequency sound at Etosha, with range at a maximum and directionality at a minimum, As the night progresses, a nocturnal low-level wind maximum (jet) forms, reducing upwind range and calling area, The estimated calling area drops rapidly after sunrise with the destruction of the inversion, Daytime calling areas are usually less than 50 km(2), while early evening calling areas frequently exceed 200 km(2) and are much less directional, This marked diurnal cycle will be present in any dry savanna climate, with variations due to local topography and climate, Calling range and low-frequency sound propagation cannot be effectively understood without knowledge of meteorological controls DA - 1997-03 DB - ResearchSpace DP - CSIR KW - Elephant infrasound propagation KW - African Elephants KW - Boundary layer profiles KW - Estosha National Park KW - Namibia LK - https://researchspace.csir.co.za PY - 1997 SM - 0001-4966 T1 - Meteorology and elephant infrasound at Etosha National Park, Namibia TI - Meteorology and elephant infrasound at Etosha National Park, Namibia UR - http://hdl.handle.net/10204/2145 ER -